胡国艺,张水昌,田 华,陈建平,田兴旺,王飞宇,马行陟
HU Guo-yi,ZHANG Shui-chang,TIAN Hua,CHEN Jian-ping,TIAN Xing-wang,WANG Fei-yu,MA Xing-zhi
摘要:
随着全球页岩气等非常规油气勘探的不断加强,烃源岩排气效率的研究越来越受到关注。根据页岩或煤中实测或理论计算的含气量数据,以及在不同热演化阶段的生气量,探讨了不同母质类型烃源岩在不同热演化阶段的排气效率。煤系烃源岩和海相Ⅰ—Ⅱ1型烃源岩排气效率随着成熟度的增加,排气效率逐渐增加,但两者存在很大的差异,煤系烃源岩排气效率很高,在RO=1.0%时为75%,在RO=5.5%时高达90%以上,高排气效率表明,煤系烃源岩生成的天然气绝大部分都运移到了储层,成为常规天然气和致密砂岩气的主要气源。与煤系烃源岩相比,海相Ⅰ—Ⅱ1型烃源岩排气效率较低,大部分低于70%,低排气效率结果表明,在页岩体系中生成的天然气相当一部分仍滞留在烃源岩中,残留在页岩中的天然气为页岩气的富集提供了物质基础。
中图分类号:
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